update........on Computational computability
Two Methods....of....physical modelling solid solution surfaces
.......1:Deterministic (classical-reversible TIME points)
..........'versus'
.......2: in-Deterministic (20^th century-ireversible TIME points)
note.....both
1: and 2: ....are factorable by pairs Gibb's free energy boundary line
endpoints G[Joule] with length R[m] that satisfy Gauss's Volume Integral
formulae
looks ok.....anyone else may
suggest..........on how 1: and 2: can be extended to a 21^st Gibb's free
energy model that includes a vacuum energy state?
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